ペロポネソス山脈の天然記念物・トップ20

アギオス・ニコラオス・グルナ地方と隣接するヴライコス渓谷の岩壁は、地質学的に非常に特徴的です。 ここの岩石は主に2つのタイプで構成されています。 赤い礫岩：これらは特に顕著で、多くの岩壁に特徴的な粗い構造と赤みを帯びた色を与えています。礫岩は、細かい基質によって「接合」された丸みを帯びた岩石の破片（小石など）で構成される堆積岩です。 石灰岩：この地域が属するチェルモス・ヴライコスユネスコ世界ジオパークの大部分は、石灰岩で構成されています。これはしばしば強くカルスト化されており、渓谷の多くの洞窟や印象的な岩石層の形成に貢献しています。

Very interesting, much more interesting to show us electric bikes than to show us the crater. When will people start giving real information?

Methana Peninsula The Methana Peninsula was formed from the seabed by successive volcanic eruptions that began about 1,000,000 years ago and ended about 250,000 years ago. Then everything was quiet here for thousands of years and the landscape we see today was already formed. However, around 250 BC there was another small eruption. This eruption is mentioned by Pausanias, among others, in his writings. He says that there was a fertile plain that stretched from the present village of Kammeni Chora to the sea in the west. The whole area was covered by lava that accumulated over months and formed the steep mountain that you can see right behind your back. The height of the mountain is about 400 m. It was not a violent eruption. During the last phase, the viscous lava flow died out in the sea in the west. The volcanoes of Methana do not have the typical caldera shape. The lava here was so viscous that it accumulated vertically, forming high, steep mountains. The eruptions here were usually not violent and lasted a long time. In general, every mountain you see in the area is a single eruption. About 30 individual volcanic eruptions are visible on the Methana peninsula. On the summit of Kammeni Chora volcano you will find a crack that probably appeared during the last phase of the eruption, when the rich lava flow reached the sea. From the summit you can follow the lava flow with your eyes all the way to the sea. The sunset here is more beautiful than on Santorini. The lava glows red again in the last light of the setting sun. Methana volcano is active, however we cannot yet predict where and when the next eruption will be. The hike to the summit takes about 25 minutes. Text and pictures: Elias Rizos - www.volcanotrails.gr Read about the Kammeni Chora volcano on www.volcanotrails.gr SCAN ME A travel guide to Methana-topia www.volcanotrails.gr SCAN ME Map of Methe Background from 2002 Methana Peninsula The Methana peninsula was formed from the seabed by successive volcanic eruptions that began about 1,000,000 years ago and ended about 250,000 years ago. Then everything was quiet here for thousands of years and the landscape we see today was already formed. However, around 250 BC there was another small eruption. This eruption is mentioned by Pausanias, among others, in his writings. He says that there was a fertile plain that stretched from the present village of Kammeni Chora to the sea in the west. The whole area was covered by lava, which accumulated for months and formed the steep mountain that you can see right behind your back. The height of the mountain is about 400 m. It was not a violent eruption. During the last phase, the viscous lava flow died out in the sea to the west. Methana's volcanoes do not have the typical caldera shape. The lava here was so viscous that it accumulated vertically and formed high, steep mountains. The eruptions here were usually not violent and lasted a long time. In general, every mountain you see in the area is a single eruption. About 30 individual volcanic eruptions are visible on the Methana peninsula. On the summit of the Kammeni Chora volcano you will find a crack that probably appeared during the last phase of the eruption, when the rich lava flow reached the sea. From the summit you can follow the lava flow with your eyes all the way to the sea. The sunset here is more beautiful than on Santorini. The lava glows red again in the last light of the setting sun. Methana volcano is active, however we cannot yet predict where and when the next eruption will be. The hike to the top takes about 25 minutes. Text and pictures: Elias Rizos – www.volcanotrails.gr Read about Kammeni Chora volcano on www.volcanotrails.gr SCAN ME A travel guide to Methana-topia www.volcanotrails.gr SCAN ME Map of Methe Background from 2002 Με χρώματα στp

Next to the old stone bridge is the exit point from the Neda Gorge to reach the waterfalls.

The waterfall directly at the stone bridge is not the highlight; the more beautiful ones come later on the tour.

The bathroom has been completely renovated and now has an outdoor pool - the bathhouse itself has been closed since a suffocation accident. All you have to do is press a green button and a pump starts filling the pool for 15 minutes. If you want to bathe longer, simply press the button again. In January 2024 the water had a temperature of around 30 degrees.

Currently, Nov. 23, the path over the bridge is closed due to a landslide, but can be done at your own risk.

The bridge can be reached from both sides by MTB. The up-and-down route is still mobile at a maximum of 16%.